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Haiti Earthquake Mw7.0

 
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Update Number: Final Summary

Cat Date: 1/12/2010

Posting Date: 1/22/2010
 

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Characteristics

Mw 7.0 Mainshock
On Tuesday, 12 January at 21:53 UTC (04:53 pm local time) a powerful magnitude 7.0 (moment magnitude, Mw) earthquake occurred in south Haiti, close to the capital of Port-au-Prince. The USGS have determined a fixed shallow depth estimate of 8.1 miles (13 km) and an epicentral location of 18.457N 72.533W, approximately 15 miles (25 km) west-southwest of Port-au-Prince, Haiti; 80 miles (130 km) east of Les Cayes, Haiti; and 700 miles (1125 km) southeast of Miami, USA.

The earthquake was widely felt across Haiti, the Dominican Republic, the southeast Bahamas, Jamaica and the northeast and southeast coasts of Cuba. According to the USGS Shakemap, the region of Ouest department, to the west and northwest of the epicentre, experienced the highest intensity, violent shaking (up to IX on the Modified Mercalli Intensity, MII, scale) which has the potential to cause heavy damage to property. Regions of the departments of Ouest, Sud-est and Nippes would also have experienced severe shaking (MMI VIII) which has the potential to cause moderate-to-heavy damage. The two cities closest to the epicentre are Port-au-Prince (population 1.1 million) and Jacmel (population 40,000) experienced up to intensity VII (very strong) shaking on the MMI scale according to ShakeMap. This intensity of shaking can be expected to cause moderate damage to property.

Following the earthquake, the NOAA/NWS/West Coast and Alaska Tsunami Warning Center indicated that a strong earthquake had occurred, but a tsunami was not expected along the coasts of Puerto Rico, the Virgin Islands, U.S. Atlantic and Gulf of Mexico states, and Eastern Canadian provinces. In addition, no tsunami warning, watch or advisory was put in place for these areas. An initial tsunami warning was issued for the Caribbean region by the Pacific Tsunami Warning Center, and then cancelled shortly thereafter. According to the NOAA, a tsunami measuring 4.7 inches (12 cm) crest-to-trough was recorded at Santo Domingo, Dominican Republic and a tsunami with less than 0.4 inches (1 cm) crest-to-trough was recorded on a deep ocean gauge in the east-central Caribbean.

Tectonic Setting
This earthquake occurred in the boundary region that separates the Caribbean and North America tectonic plates. The predominant styles of deformation in this area are left-lateral strike-slip fault motions and compression; together they accommodate some 0.8 inches/yr (20 mm/yr) of slip as the Caribbean plate moves eastwards with respect to the North America plate.

Fault plane solutions calculated in the aftermath of this event by the USGS and other agencies indicate that the mechanism of the earthquake is consistent with having occurred as left-lateral strike-slip faulting on the Enriquillo-Plaintain Garden fault system in southern Haiti. This is a major east-west trending strike-slip fault system which accommodates approximately 0.3 inches/yr (7mm/yr) of the motion between the Caribbean and North America plates.

The Enriquillo-Plaintain Garden fault system has not generated a major earthquake in recent decades. It is thought that this system is the likely source of the large earthquakes in 1860, 1770, 1761, 1751, 1684, 1673, and 1618, though none of these events have been directly confirmed in the field.

Aftershocks
By 10:00 UTC on Friday, 22 January there had been 54 aftershock of Mw 4.0 or greater in the vicinity of the Mw7.0 mainshock; the vast majority occurring to the west of the mainshock.

The USGS has reported that the two largest aftershocks both measured Mw5.9. The first of these occurred at 22:00 UTC (5:00 pm local time) on Wednesday, 13 January, several minutes after the mainshock. This aftershock was assigned a fixed focal depth of 6.2 miles (10 km) by the USGS and an epicentral location of 18.36N 72.82W, approximately 20 miles (30 km) west-southwest of the mainshock. The second Mw5.9 aftershock occurred at 11:03 UTC on Wednesday, 20 January, eight days after the mainshock. The USGS reported a fixed focal depth of 6.2 miles (10 km) and an epicentral location of 18.425N, 72.805W, approximately 18 miles (29 km) west of the mainshock. The location of this second Mw5.9 aftershock is shown on the location map at the top of this page.

According to the USGS shakemap, both of these large aftershocks could have caused up to intensity V (moderate) shaking on the MMI scale in the region of Port-au-Prince. Typically, this amount of shaking would be expected to cause very light damage to property; however in the aftermath of a large earthquake that has significantly weakened an already vulnerable building stock, it could be expected that aftershocks of this size would be responsible for additional property damage.

For more information about the characteristics of this event, please read the RMS Haiti Earthquake FAQ.
 
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Summary

 
 

All Cat Updates for this Event

Update #1 (1/13/2010)
Final Summary (1/22/2010)

Related Information

Additional Web Resources
 
     

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